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Gas chromatography of gas samples of the KTB pilot hole VB1a
The main objective of this drilling fluid analysis was the detection of inflows of formation fluids. Therefore different gases dissolved in the drilling mud were measured... -
Gas Mass Spectrometry of Gas Samples of the KTB Pilot Hole VB1a
In the complete KTB-VB and in in the KTB-HB down to a depth of 3003 m the gas phase was released and collected by twirl degassers attached in front of the mud shakers. This open... -
Age determination of sediment core BDP96-1(BDP-2-A)
Two boreholes, one to a depth of 300 m, and the other to a depth of 100 m below sediment surface were drilled at 53°41´48´´N-108°21´06´´E. The core was collected down to 200m in... -
Percent DW and %LOI values for the surface sediment core taken at site BAIK38...
Samples were routinely analysed for wet density (WD), percentage dry weight (%DW) at 105 °C, and loss-on-ignition analysis (LOI) at 550 °C, and data used to calculate diatom... -
Gas mass spectrometry of gas samples from the KTB Main Hole HB1
The main objective of this drilling fluid analysis was the detection of inflows of formation fluids. Therefore different gases dissolved in the drilling mud were measured... -
Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1 (measurements...
In the laboratory, the gamma radiation is measured by a sodium iodtite (NaI) scintillation detector (cores and cuttings) and by a germanium (Ge) semiconductor detector... -
Density of Cuttings of the KTB Pilot Hole Vb1
The density of rocks depends on the mineral contents and is therefore a helpful property for the discrimination of lithological units. It is also used for the calculation of... -
Thermal Conductivity of Cores of the KTB Pilot Hole VB1a (transformed data)
The thermal conductivity on cores is measured in two steps (see Pribnow 1994). First, one face end of the core is sawed and polished. The half space line source is pressed... -
Raw pollen data from the Eemian core CON01-603-2
The studied core CON01-603-2 was recovered from the Continent site, Northern Basin from a water depth of 386 m (Fig. 1) (see Charlet et al., 2005-this volume). The analysed... -
Major composition (wt.%) of concretions, ICP-AES measurements
In order to get a complete geochemical signature, 14 P-rich concretions, chosen among the different cores, were acid digested (Table 3a and Table 3b). In a clean laboratory, 1.7... -
Permeability of Mini Cores of the KTB Pilot Hole VB1: Instationary Measurements
In the KTB field laboratory, porosity, internal surface and permeability were determined on identical mini cores with 25.4 mm in diameter and approximately 50 mm in length.... -
Natural Gamma-ray Activity of Cuttings of the KTB Main Hole HB1d (measurement...
In the laboratory, the gamma radiation is measured by a sodium iodtite (NaI) scintillation detector (cores and cuttings) and by a germanium (Ge) semiconductor detector... -
SAFOD Main Hole downhole logging data phase 1.2 1368-1556m
SAFOD is motivated by the need to answer fundamental questions about the physical and chemical processes controlling faulting and earthquake generation within a major... -
XRD of Cores of the KTB Main Hole HB1d
The qualitative and quantitative phase analyses were performed in the KTB field laboratory by x-ray powder diffraction using SIEMENS D 500 diffractometer. During early stages of... -
Downcore variations of the water content for the sedimentary sequence of VER ...
The water content was determined from samples retrieved with cylindrical syringe samplers, weighed wet and weighed again after freeze-drying. The clay-rich layers are... -
Thermal Conductivity of Cores of the KTB Pilot Hole VB1 (transformed data)
The thermal conductivity on cores is measured in two steps (see Pribnow 1994). First, one face end of the core is sawed and polished. The half space line source is pressed... -
Depth versus age based on relative magnetic paleointensity correlations for a...
In order to characterise Lake Baikal sedimentary responses to global climatic changes that may be recorded in marine sediments, we compared our paleomagnetically dated... -
Diatom record (in relative percentages) and the biovolume accumulation rates ...
The diatom succession at Academician Ridge is similar to the one from Continent Ridge and the two records, despite having very different sampling resolution, can be easily... -
Geochemistry of sediment core BDP-2-A ( BDP96-1) from Lake Baikal
Geochemistry of sediment core BDP-2-A ( BDP96-1) from Lake Baikal -
XRF of Centrifuge Samples of the KTB Pilot Hole VB1.
Cuttings were crushed in a tungsten carbide ball mill for 25 min; while core samples were crushed in a tungsten carbide jaw breaker and then processed in the same way as the...
